The Zitacuaro Volcanic Complex, Michoacan, Mexico: magmatic and eruptive history of a resurgent caldera

The Zitacuaro Volcanic Complex (ZVC) rises on a basement of metamorphic rocks of Late Jurassic-Early Cretaceous age, and volcanic rocks, limestones, and red beds of Cretaceous age. Volcanic activity related to the Trans-Mexican Volcanic Belt started during Early Miocene with the eruption of calc-alk...

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Detalhes bibliográficos
Autores: Capra, Lucia, Macías-Vázquez, José Luis, Garduño-Monroy, Victor Hugo
Tipo de documento: artigo
Estado:Versão publicada
Data de publicação:1997
País:México
Recursos:UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO
Repositório:Geofísica Internacional
Idioma:espanhol
OAI Identifier:oai:revistagi.geofisica.unam.mx:article/633
Acesso em linha:http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/633
Access Level:Acceso aberto
Palavra-chave:Cinturón volcánico mexicano
caldera
, resurgencia dómica
Trans-Mexican volcanic belt
resurgent domes
Descrição
Resumo:The Zitacuaro Volcanic Complex (ZVC) rises on a basement of metamorphic rocks of Late Jurassic-Early Cretaceous age, and volcanic rocks, limestones, and red beds of Cretaceous age. Volcanic activity related to the Trans-Mexican Volcanic Belt started during Early Miocene with the eruption of calc-alkaline andesites that formed a primitive stratovolcano covering an area about 30 km x 15 km. A major change in eruptive style occurred during Middle Miocene, when a caldera structure formed, "Las Tres Chicas Caldera", approximately 30 km in diameter and dated about 12 Ma. Post-caldera activity consisted of three eruptive episodes of intra-caldera dome resurgence around 12 Ma, 5 Ma, and 0.5 Ma. Each episode featured the intrusion of dacitic central domes, the generation of pyroclastic flows and peri-caldera andesitic lava flows. The activity at the ZVC features recurrent volcanic episodes, the most recent one with emplacement of young resurgent domes such as Cacique. Local seismic activity in the area felt at Zitacuaro, is persistent. The ZVC should be considered as a potentially active volcanic zone.